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南极普里兹湾表层沉积物有机地球化学特征及其生态环境意义
引用本文:赵军,于培松,韩正兵,扈传昱,潘建明.南极普里兹湾表层沉积物有机地球化学特征及其生态环境意义[J].极地研究,2014,26(1):167-174.
作者姓名:赵军  于培松  韩正兵  扈传昱  潘建明
作者单位:1.国家海洋局海洋生态系统和生物地球化学重点实验室,,浙江 杭州 310012; ;2.国家海洋局第二海洋研究所,浙江 杭州 310012
基金项目:国家自然科学基金项目(41376193,41306202,41006118,41076134,40876104);国家海洋局第二海洋研究所基本科研业务费专项(JT1208,JG1218);中国极地科学战略研究基金项目(20110208);南北极环境综合考察与评估专项(CHINARE2013-01-04)资助
摘    要:用气相色谱和气相色谱-质谱分析法分析了南极普里兹湾5个站位表层沉积物中多种生物标志物,探讨了其生态环境指示意义。结果显示:(1)湾内中心区总类脂物含量最高(1 193μg·g-1),埃默里冰架区次之(572μg·g-1),陆坡区最低(341μg·g-1),且与沉积有机碳、总糖、生物硅、菜籽甾醇、表层海水叶绿素a等参数显著正相关(p0.1),表明底层有机质与上层水体浮游植物密切相关;(2)C27甾烷含量与C28甾烷显著负相关(p0.01),指示着晶磷虾与硅藻的食物链关系;(3)相对较高的饱和烃/芳烃比值(2.5)、较低的Pr/C17(0.5)和Pr/Ph(2)证明沉积有机质主要来源于硅藻等浮游植物,同时饱和烃双峰群(C17或C18和C29)的存在及较高含量的C29甾烷(35.79%)指示外域有机质输入,且湾中心区的(CPI=1.60,Pr/Ph=0.69)要高于陆坡区和冰架区(CPI=1.01,Pr/Ph=0.39);(4)湾内中心区和冰架区脂肪酸C18:2/C18:0平均比值(0.78)要高于陆坡区(0.23)和低纬度地区(0.1),表明南极夏季普里兹湾陆坡区的表层海水温度要高于湾中心区和冰架区。

关 键 词:普里兹湾  生物标志物  表层沉积物  生态环境  

ORGANIC GEOCHEMICAL CHARACTERISTICS OF SURFACE SEDIMENTS AND IMPLICATIONS FOR ECOLOGY AND ENVIRONMENT IN PRYDZ BAY,ANTARCTICA
Zhao Jun,Yu Peisong,Han Zhengbing,Hu Chuanyu,Pan Jianming.ORGANIC GEOCHEMICAL CHARACTERISTICS OF SURFACE SEDIMENTS AND IMPLICATIONS FOR ECOLOGY AND ENVIRONMENT IN PRYDZ BAY,ANTARCTICA[J].Chinese Journal of Polar Research,2014,26(1):167-174.
Authors:Zhao Jun  Yu Peisong  Han Zhengbing  Hu Chuanyu  Pan Jianming
Institution:1.Key Laboratory of Marine Ecosystem and Biogeochemistry, SOA, Hangzhou 310012, China;2.Second Institute of Oceanography, SOA, Hangzhou 310012, China
Abstract:Multiple biomarkers has been analyzed by gas chromatography and gas chromatography – mass spectrum on surface sediments collected from 5 stations in Prydz Bay, East Antarctica, and its implication on ecology and environment has been discussed. The results showed that the concentration of total lipids was highest in the center area of Prydz Bay (1193 µg/g), follow by Amery Ice Shelf area (572 µg/g), and lowest in slope area (341 µg/g). It was significantly positive correlated with sedimentary organic carbon, total neutral monosaccharides, biogenic silica, brassicasterol, and chlorophyll a concentrations in surface sea water (p < 0.1), and indicated that organic matter preserved in surface sediment was mainly from marine phytoplankton. The significantly negative correlation of relative concentrations between C27 and C28 steranes showed the food chain between Euphausia crystallorophias and diatoms. The relative high ratio of saturated hydrocarbons : arenes (> 2.5), low ratios of Pr/C17 (< 0.5) and Pr/Ph (< 2) inferred the sedimentary organic matter was largely contributed by diatoms. Meanwhile, the double peak of saturated hydrocarbons (C17 or C18, C29) and relative high concentration of C29 steranes (35.79%) showed terrestrial vascular plants input, and it was higher in the center area of Prydz Bay (CPI = 1.60, Pr/Ph = 1.01) than the slope area and Amery Ice Shelf area (CPI = 0.69, Pr/Ph = 0.39). The ratio of C18:2/C18:0 for fatty acids was higher in sediment collected from the center area and Amery Ice Shelf area of Prydz Bay (0.78) than that from slope area of Prydz Bay (0.23) and lower latitude regions (< 0.1), and indicated that during austral summer, the surface sea temperature was higher in slope area of Prydz Bay than center area of Prydz Bay and Amery Ice Shelf area.
Keywords:Prydz Bay  biomarker  surface sediment  ecology and environment  
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